Abstract
We developed a 378-year tree-ring-width chronology based on 110 core samples from 55 individual trees of Larix gmelinii (Rupr.) Rupr. growing in a wide open forest close to the tree line in the Kronotsky National Park. Reflecting strong climatic control over tree growth not only within the study area but also more extensively over central Kamchatka, our chronology was well correlated with those from other larch sites. Response analysis with 10-day mean temperature revealed that the ring width was primarily controlled by the temperature of early summer, i.e., of late May through late June (40 days). While the regression models for a formal reconstruction failed to pass stringent verification tests commonly used in dendroclimatology, the relationship between tree growth and climate was statistically significant and credible. We therefore used our chronology as a proxy of early summer temperature. The chronology shows a cool period from the 1660s until the 1680s, followed by gradual warming until ca. 1800, then by a slight cooling trend extending to ca. 1910, and a warming trend continuing up to the present, with decadal fluctuations throughout the chronology. The warming trend found in our chronology over the twentieth century is generally consistent with the ones commonly appearing in higher latitudes.
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Acknowledgments
We thank Y.D. Muravyev for his assistance in our sample collection in Kamchatka. We are also grateful to M. Yamano and T. Nagao for inviting us to this study as a part of their paleoclimate reconstruction project primarily based on inversion of borehole temperature profiles. We also thank three anonymous reviewers for valuable comments and suggestions for improving this manuscript. This study was funded by the 2000–2002 Grant-in-Aid for Overseas Scientific Research (B) 12573015 from the Ministry of Education, Culture, Sports, Science and Technology, Japan.
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Sano, M., Furuta, F. & Sweda, T. Tree-ring-width chronology of Larix gmelinii as an indicator of changes in early summer temperature in east-central Kamchatka. J For Res 14, 147–154 (2009). https://doi.org/10.1007/s10310-009-0123-y
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DOI: https://doi.org/10.1007/s10310-009-0123-y